固原体应变观测资料综合分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
对固原海子峡体应变2008年1月以来的观测数据进行了连续率、日漂移、内在精度以及噪声水平等方面的统计分析,结果显示观测资料连续率高,内在精度高,漂移快,噪声水平相对偏高。并从中选取了4个时段与气压进行相关分析,结果显示两者存在高度相关性,且体应变随气压变化在时间上存在40 min的滞后效应,应用相关分析方法去除气压对体应变的影响,能通过资料内精度检验,效果显著。结合宁夏南部地区震情趋势,应用差分分析方法简要介绍了4级左右地震前体应变出现的异常变化特征。
The statistical analysis of volume strain data since January in 2008 in Guyuan station was done,including continue rate,daily drift,intrinsic accuracy and noise level etc.The result showed the continue rate,intrinsic accuracy and noise level were all higher,the daily drift was fast.The correlation analysis between the observation data and barometric pressure was done during 4 selected periods and the result showed the observation data was closely related with barometric pressure and there was hysteresis effect for 40 minutes.Removing barometric pressure influence through correlation analysis could pass the intrinsic accuracy test and got significant effects.Combined with earthquake tendency in south of Ningxia,the anomaly characteristics before 4.0 earthquakes was introduced using difference analysis briefly.
引文
[1]李杰,刘敏,邹钟毅,等.数字化钻孔体应变干扰机理及异常分析[J].地震研究,2006,26(3):230-238.
    [2]张学阳.潮汐观测中高精度气压辅助观测的必要性及气压效应改正[J].地壳形变与地震,1987,4(4):273-280.
    [3]王梅.数字化体应变与气压、水位相关性研究[J].大地测量与地球动力学,2002,22(4):85-88.
    [4]林纪曾.观测数据的数学处理[M].北京:地震出版社,1981.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心